Classical Kuiper belt object

The orbits of various cubewanos compared to the orbit of Neptune (blue) and Pluto (pink)

A classical Kuiper belt object, also called a cubewano (/ˌkjuːbˈwʌn/ "QB1-o"),[1] is a low-eccentricity Kuiper belt object (KBO) that orbits beyond Neptune and is not controlled by an orbital resonance with Neptune. Cubewanos have orbits with semi-major axes in the 40–50 AU range and, unlike Pluto, do not cross Neptune’s orbit. That is, they have low-eccentricity and sometimes low-inclination orbits like the classical planets.

The name "cubewano" derives from the first trans-Neptunian object (TNO) found after Pluto and Charon, (15760) 1992 QB1.[2] Similar objects found later were often called "QB1-o's", or "cubewanos", after this object, though the term "classical" is much more frequently used in the scientific literature.

Objects identified as cubewanos include:

Haumea was provisionally listed as a cubewano by the Minor Planet Center in 2006,[4] but turned out to be resonant.[3]

The orbits of the large cubewanos (in blue) with the large resonant trans-Neptunian objects (including plutinos) (in red) for comparison (H<4.5). The horizontal axis represents the semi-major axes. The eccentricities of the orbits are represented by segments (extending from perihelion to aphelion) with the inclinations represented on the vertical axis.

Orbits: 'hot' and 'cold' populations

Most cubewanos are found between the 2:3 orbital resonance with Neptune (populated by plutinos) and the 1:2 resonance. 50000 Quaoar, for example, has a near-circular orbit close to the ecliptic. Plutinos, on the other hand, have more eccentric orbits bringing some of them closer to the Sun than Neptune.

The majority of objects (the so-called 'cold population'), have low inclinations and near-circular orbits. A smaller population (the 'hot population') is characterised by highly inclined, more eccentric orbits.[5]

The Deep Ecliptic Survey reports the distributions of the two populations; one with the inclination centered at 4.6° (named Core) and another with inclinations extending beyond 30° (Halo).[6]


This diagram plots the distribution of cubewanos and resonant TNOs (including plutinos).

The vast majority of KBOs (more than two-thirds) have inclinations of less than 5° and eccentricities of less than 0.1. Their semi-major axes show a preference for the middle of the main belt; arguably, smaller objects close to the limiting resonances have been either captured into resonance or have their orbits modified by Neptune.

The 'hot' and 'cold' populations are strikingly different: more than 30% of all cubewanos are in low inclination, near-circular orbits. The parameters of the plutinos’ orbits are more evenly distributed, with a local maximum in moderate eccentricities in 0.15–0.2 range and low inclinations 5–10°. See also the comparison with scattered disk objects.

Polar and ecliptic view of the (aligned) orbits of the classical objects (in blue), together with the plutinos in red, and Neptune (yellow).

When the orbital eccentricities of cubewanos and plutinos are compared, it can be seen that the cubewanos form a clear 'belt' outside Neptune's orbit, whereas the plutinos approach, or even cross Neptune's orbit. When orbital inclinations are compared, 'hot' cubewanos can be easily distinguished by their higher inclinations, as the plutinos typically keep orbits below 20°. (No clear explanation currently exists for the inclinations of 'hot' cubewanos.[7])

Cold and hot populations: physical characteristics

In addition to the distinct orbital characteristics, the two populations display different physical characteristics.

The difference in colour between the red cold population and more heterogeneous hot population was observed as early as in 2002.[8] Recent studies, based on a larger data set, indicate the cut-off inclination of 12° (instead of 5°) between the cold and hot populations and confirm the distinction between the homogenous red cold population and the bluish hot population.[9]

Another difference between the low-inclination (cold) and high-inclination (hot) classical objects is the observed number of binary objects. Binaries are quite common on low-inclination orbits and are typically similar-brightness systems. Binaries are less common on high-inclination orbits and their components typically differ in brightness. This correlation, together with the differences in colour, support further the suggestion that the currently observed classical objects belong to at least two different overlapping populations, with different physical properties and orbital history.[10]

Toward a formal definition

There is no official definition of 'cubewano' or 'classical KBO'. However, the terms are normally used to refer to objects free from significant perturbation from Neptune, thereby excluding KBOs in orbital resonance with Neptune (resonant trans-Neptunian objects). The Minor Planet Center (MPC) and the Deep Ecliptic Survey (DES) do not list cubewanos (classical objects) using the same criteria. Many TNOs classified as cubewanos by the MPC are classified as ScatNear (possibly scattered by Neptune) by the DES. Dwarf planet Makemake is such a borderline classical cubewano/scatnear object. (119951) 2002 KX14 may be an inner cubewano near the plutinos. Furthermore, there is evidence that the Kuiper belt has an 'edge', in that an apparent lack of low-inclination objects beyond 47–49 AU was suspected as early as 1998 and shown with more data in 2001.[11] Consequently, the traditional usage of the terms is based on the orbit’s semi-major axis, and includes objects situated between the 2:3 and 1:2 resonances, that is between 39.4 and 47.8 AU (with exclusion of these resonances and the minor ones in-between).[5]

These definitions lack precision: in particular the boundary between the classical objects and the scattered disk remains blurred. As of 2010, there are 377 objects with perihelion (q) > 40 AU and aphelion (Q) < 47 AU.[12]

DES classification

Introduced by the report from the Deep Ecliptic Survey by J. L. Elliott et al. in 2005 uses formal criteria based on the mean orbital parameters.[6] Put informally, the definition includes the objects that have never crossed the orbit of Neptune. According to this definition, an object qualifies as a classical KBO if:

SSBN07 classification

An alternative classification, introduced by B. Gladman, B. Marsden and C. van Laerhoven in 2007, uses a 10-million-year orbit integration instead of the Tisserand's parameter. Classical objects are defined as not resonant and not being currently scattered by Neptune.[13]

Formally, this definition includes as classical all objects with their current orbits that

Unlike other schemes, this definition includes the objects with major semi-axis less than 39.4 AU (2:3 resonance)—termed inner classical belt, or more than 48.7 (1:2 resonance) – termed outer classical belt, and reserves the term main classical belt for the orbits between these two resonances.[13]


The first known collisional family in the classical Kuiper belt—a group of objects thought to be remnants from the breakup of a single body—is the Haumea family.[14] It includes Haumea, its moons, 2002 TX300 and seven smaller bodies. The objects not only follow similar orbits but also share similar physical characteristics. Unlike many other KBO their surface contains large amounts of ice (H2O) and no or very little tholins.[15] The surface composition is inferred from their neutral (as opposed to red) colour and deep absorption at 1.5 and 2. μm in infrared spectrum.[16]

As of 2008. The four brightest objects of the family are situated on the graphs inside the circle representing Haumea.

List of objects

Here is a very generic list of classical Kuiper belt objects. As of 2014, there are about 473 objects with q > 40 (AU) and Q < 48 (AU).


  1. Somewhat old-fashioned, but still used by the Minor Planet Center for their list of Distant Minor Planets
  2. David Jewitt. "Classical Kuiper Belt Objects". David Jewitt/UCLA. Retrieved July 1, 2013.
  3. 1 2 3 4 Brian G. Marsden (2010-01-30). "MPEC 2010-B62 : Distant Minor Planets (2010 FEB. 13.0 TT)". IAU Minor Planet Center. Harvard-Smithsonian Center for Astrophysics. Retrieved 2010-07-26.
  4. "MPEC 2006-X45 : Distant Minor Planets". IAU Minor Planet Center & Tamkin Foundation Computer Network. 2006-12-12. Retrieved 2008-10-03.
  5. 1 2 Jewitt, D.; Delsanti, A. (2006). "The Solar System Beyond The Planets". Solar System Update : Topical and Timely Reviews in Solar System Sciences. Springer-Praxis. ISBN 3-540-26056-0. (Preprint Archived January 29, 2007, at the Wayback Machine.)
  6. 1 2 J. L. Elliot; et al. (2006). "The Deep Ecliptic Survey: A Search for Kuiper Belt Objects and Centaurs. II. Dynamical Classification, the Kuiper Belt Plane, and the Core Population". Astronomical Journal. 129 (2): 1117. Bibcode:2005AJ....129.1117E. doi:10.1086/427395. (Preprint)
  7. Jewitt, D. (2004). "Plutino".
  8. A. Doressoundiram; N. Peixinho; C. de Bergh; S. Fornasier; P. Thebault; M. A. Barucci; C. Veillet (October 2002). "The Color Distribution in the Edgeworth-Kuiper Belt". The Astronomical Journal. 124 (4): 2279. arXiv:astro-ph/0206468Freely accessible. Bibcode:2002AJ....124.2279D. doi:10.1086/342447.
  9. Nuno Peixinho; Pedro Lacerda; David Jewitt (August 2008). "Color-inclination relation of the classical Kuiper belt objects". The Astronomical Journal. 136 (5): 1837. arXiv:0808.3025Freely accessible. Bibcode:2008AJ....136.1837P. doi:10.1088/0004-6256/136/5/1837.
  10. K. Noll; W. Grundy; D. Stephens; H. Levison; S. Kern (April 2008). "Evidence for two populations of classical transneptunian objects: The strong inclination dependence of classical binaries". Icarus. 194 (2): 758. arXiv:0711.1545Freely accessible. Bibcode:2008Icar..194..758N. doi:10.1016/j.icarus.2007.10.022.
  11. Trujillo, Chadwick A.; Brown, Michael E. (2001). "The Radial Distribution of the Kuiper Belt" (PDF). The Astrophysical Journal. 554: L95. Bibcode:2001ApJ...554L..95T. doi:10.1086/320917.
  12. "JPL Small-Body Database Search Engine". JPL Solar System Dynamics. Retrieved 2010-07-26.
  13. 1 2 Gladman, B. J.; Marsden, B.; van Laerhoven, C. (2008). "Nomenclature in the Outer Solar System". In Barucci, M. A.; et al. The Solar System Beyond Neptune (PDF). Tucson: University of Arizona Press. ISBN 978-0-8165-2755-7.
  14. Brown, Michael E.; Barkume, Kristina M.; Ragozzine, Darin; Schaller, Emily L. (2007). "A collisional family of icy objects in the Kuiper belt". Nature. 446 (7133): 294–6. Bibcode:2007Natur.446..294B. doi:10.1038/nature05619. PMID 17361177.
  15. Pinilla-Alonso, N.; Brunetto, R.; Licandro, J.; Gil-Hutton, R.; Roush, T. L.; Strazzulla, G. (2009). "The surface of (136108) Haumea (2003 EL61), the largest carbon-depleted object in the trans-Neptunian belt". Astronomy and Astrophysics. 496 (2): 547. arXiv:0803.1080Freely accessible. Bibcode:2009A&A...496..547P. doi:10.1051/0004-6361/200809733.
  16. Pinilla-Alonso, N.; Licandro, J.; Gil-Hutton, R.; Brunetto, R. (2007). "The water ice rich surface of (145453) 2005 RR43: a case for a carbon-depleted population of TNOs?". Astronomy and Astrophysics. 468: L25. arXiv:astro-ph/0703098Freely accessible. Bibcode:2007A&A...468L..25P. doi:10.1051/0004-6361:20077294.

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